Oscillations with a period of 5.6 min were observed on 10 July, 1978 while tracking at 22 GHz the active region McMath 15403. The oscillations were strong, clearly defined, had no damping, and lasted for about two hours. The rarity of the phenomenon is indicated by the fact that it occurred only onc
Five-minute oscillations of solar equivalent widths
โ Scribed by Hartmut Holweger; Larry Testerman
- Publisher
- Springer
- Year
- 1975
- Tongue
- English
- Weight
- 776 KB
- Volume
- 43
- Category
- Article
- ISSN
- 0038-0938
No coin nor oath required. For personal study only.
โฆ Synopsis
Equivalent widths of weak and moderately strong Fraunhofer lines observed in an area roughly 3500 โข 10000 km in extent are found to show small variations of the order of 1 mA, on a time scale of minutes. The dependence of amplitude on line strength and excitation closely fits that predicted for a compressional disturbance associated with temperature variations that manifest themselves in the equivalent widths. The rms amplitude is about 20K near r~000= 10 -2.
These equivalent width variations frequently exhibit a 5-rain periodicity and are accompanied by prominent oscillations of velocity. Power spectra of both quantities closely resemble each other and demonstrate that most of the equivalent width variations in the range 200 to 500 s are due to the thermal response of the atmosphere to 5-rain oscillations.
A systematic phase lag between velocity and equivalent width is observed, in the sense that temperature leads velocity by an average angle of 120 ~ . This deviates significantly from 90 ~ valid for standing adiabatic waves, showing that in the line-forming layers, Ts000~ 10 -2, the 5-min oscillations are markedly affected by radiative exchange.
The observed phase lag implies a radiative decay time of ~40 s, a value which agrees with modelatmosphere predictions for the line-forming layers. Since the observed wave trains frequently show constant amplitude over a much longer time, a continuous feed-back of energy seems to occur.
๐ SIMILAR VOLUMES
The acoustic overstability in a polytropic plane-parallel atmosphere with superadiabatic temperature gradient and radiative dissipation is demonstrated for optically thick disturbances. The periods of oscillation are found to be in the range 250-480 s and the associated wavelength of the order of 40
The 5-min oscillations in the photospheric velocity fields have been studied in detail from measurements on 14 absorption lines from three time sequences of spectrograms of high quality. The lines cover a range of heights in the solar atmosphere from log z = + 0.2 to --1.2. Regions oscillating coher